https://m2.mtmt.hu/ hun 2026-09-21 12:33 JournalArticle 3256462 ADMIN_APPROVED true 0 2018-07-02T22:22:11.000+0000 false 3256462 2026-08-31T13:13:43.182+0000 2018-10-10T18:35:22.573+0000 2017-08-22T13:04:30.000+0000 true 10012595 Gribovszki Katalin Eszter /api/author/10012595 Author true 10012595 2023-11-02T12:10:11.833+0000 2018-01-15T07:39:55.000+0000 true 10034548 Szabó Henriett /api/admin/10034548 Admin true 10034548 true false true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle true 10000059 Article true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle /api/subtype/10000059 Szakcikk SubType 101 true 10000059 true 1 /api/category/1 Category true 1 Gribovszki, K Estimating the upper limit of prehistoric peak ground acceleration using an in situ, intact and vulnerable stalagmite from Plavecká priepast cave (Detrekői-zsomboly), Little Carpathians, Slovakia—first results true true /api/journal/24483 REVIEWED true false 24483 false 24483 true 1383-4649 1573-157X Journal FOREIGN 21 5 1111 1130 1111 20 2017 Earthquakes hit urban centres in Europe infrequently, but occasionally with disastrous effects. Obtaining an unbiased view of seismic hazard (and risk) is therefore very important. In principle, the best way to test probabilistic seismic hazard assessments (PSHAs) is to compare them with observations that are entirely independent of the procedure used to produce PSHA models. Arguably, the most valuable information in this context should be information on long-term hazard, namely maximum intensities (or magnitudes) occurring over time intervals that are at least as long as a seismic cycle. The new observations can provide information of maximum intensity (or magnitude) for long timescale as an input data for PSHA studies as well. Long-term information can be gained from intact stalagmites in natural caves. These formations survived all earthquakes that have occurred over thousands of years, depending on the age of the stalagmite. Their ‘survival’ requires that the horizontal ground acceleration (HGA) has never exceeded a certain critical value within that time period. Here, we present such a stalagmite-based case study from the Little Carpathians of Slovakia. A specially shaped, intact and vulnerable stalagmite in the Plavecká priepast cave was examined in 2013. This stalagmite is suitable for estimating the upper limit of horizontal peak ground acceleration generated by prehistoric earthquakes. The critical HGA values as a function of time going back into the past determined from the stalagmite that we investigated are presented. For example, at the time of Jókő event (1906), the critical HGA value cannot have been higher than 1 and 1.3 m/s2 at the time of the assumed Carnuntum event (∼340 AD), and 3000 years ago, it must have been lower than 1.7 m/s2. We claimed that the effect of Jókő earthquake (1906) on the location of the Plavecká priepast cave is consistent with the critical HGA value provided by the stalagmite we investigated. 2017 145158 true true true false true false GREEN GREEN 2026-08-31 true https://doi.org/10.1007/s10950-017-9655-3 28 0 27 20 8 24 24 19 18 19 19 15 15 20 8 0 28 20 27 20 0 25 25 Folyóiratcikk Journal Article 24 24 Könyvrészlet Chapter in Book 25 0 Könyv Book 23 1 Egyéb konferenciaközlemény Conference paper 31 2 Egyéb konferenciakötet Conference proceedings 32 0 Oltalmi formák Protection forms 26 0 Disszertáció Thesis 28 1 Egyéb Miscellaneous 29 0 Alkotás Achievement 22 0 Kutatási adat Research data 33 0 Folyóiratcikk Journal Article 24 0 0 0 Könyvrészlet Chapter in Book 25 0 0 0 Könyv Book 23 0 0 0 Egyéb konferenciaközlemény Conference paper 31 0 0 0 Egyéb konferenciakötet Conference proceedings 32 0 0 0 Oltalmi formák Protection forms 26 0 0 0 Disszertáció Thesis 28 0 0 0 Egyéb Miscellaneous 29 0 0 0 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Földtudományok Osztálya HAS Section of Earth Sciences (X.) true 70 true true true A true true SjrRating 10700295 /api/sjrrating/10700295 58 0.49 journal RatingType 10002 /api/ratingtype/10002 sjr true true ClassificationExternal 1906 /api/classificationexternal/1906 true 1906 true Q2 DIRECT true true /api/publication/3256462 <div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" mtid="10012595"><a href="/gui2/?type=authors&mode=browse&sel=10012595" target="_blank">Gribovszki K (<span class="authorship-author-name">Gribovszki Katalin Eszter</span> <span class="authorAux-mtmt"> szeizmológia, térinformatika, környezettudomány</span>) </a> </span> <span class="author-affil"><span title="MTA Csillagászati és Földtudományi Kutatóközpont">MTA CSFK</span>/Geodéziai és Geofizikai Intézet</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10016343"><a href="/gui2/?type=authors&mode=browse&sel=10016343" target="_blank">Kovács K (<span class="authorship-author-name">Kovács Károly</span> <span class="authorAux-mtmt"> Geofizika</span>) </a> </span> <span class="author-affil"><span title="MTA Csillagászati és Földtudományi Kutatóközpont">MTA CSFK</span>/Geodéziai és Geofizikai Intézet</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10016841"><a href="/gui2/?type=authors&mode=browse&sel=10016841" target="_blank">Mónus P (<span class="authorship-author-name">Mónus Péter</span> <span class="authorAux-mtmt"> Szeizmológia</span>) </a> </span> <span class="author-affil"><span title="MTA Csillagászati és Földtudományi Kutatóközpont">MTA CSFK</span>/Geodéziai és Geofizikai Intézet</span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Bokelmann G </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Konecny P </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Lednická M </span> ;&nbsp;&nbsp;&nbsp; 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